Hygroscopic motions of fossil conifer cones

Zusammenfassung: Conifer cones represent natural, woody compliant structures which move their scales as passive responses to changes in environmental humidity. Here we report on water-driven opening and closing motions in coalified conifer cones from the Eemian Interglacial (approx. 126,000–113,000 years BP) and from the Middle Miocene (approx. 16.5 to 11.5 million years BP). These cones represent by far the oldest documented evidence of plant parts showing full functionality of such passive hydraulically actuated motion. The functional resilience of these structures is far beyond the biological purpose of seed dispersal and protection and is because of a low level of mineralization of the fossils. Our analysis emphasizes the functional-morphological integrity of these biological compliant mechanisms which, in addition to their biological fascination, are potentially also role models for resilient and maintenance-free biomimetic applications (e.g., adaptive and autonomously moving structures including passive hydraulic actuators)

Location
Deutsche Nationalbibliothek Frankfurt am Main
Extent
Online-Ressource
Language
Englisch
Notes
Scientific reports. Article ID 7:40302. DOI 10.1038/srep40302, issn: 2045-2322

Classification
Wirtschaft

Event
Veröffentlichung
(where)
Freiburg
(who)
Universität
(when)
2017
Creator
Contributor
Albert-Ludwigs-Universität Freiburg

DOI
10.1038/srep40302
URN
urn:nbn:de:bsz:25-freidok-115534
Rights
Der Zugriff auf das Objekt ist unbeschränkt möglich.
Last update
14.08.2025, 10:47 AM CEST

Data provider

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Associated

Time of origin

  • 2017

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